Origin of iron and aluminium in large particles (> 53 µm) in the Crozet region, Southern Ocean
Natural iron fertilization processes are occurring around the Crozet Islands (46°26?S–52°18?E), thus relieving the water masses from the normally encountered High Nutrients Low Chlorophyll (HNLC) conditions of the Southern Ocean. During austral summers 2004/2005 and 2005/2006, iron and aluminium con...
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ftsouthampton:oai:eprints.soton.ac.uk:68673 2023-08-27T04:09:07+02:00 Origin of iron and aluminium in large particles (> 53 µm) in the Crozet region, Southern Ocean Planquette, Hélène Fones, Gary R. Statham, Peter J. Morris, Paul J. 2009-06-20 https://eprints.soton.ac.uk/68673/ unknown Planquette, Hélène, Fones, Gary R., Statham, Peter J. and Morris, Paul J. (2009) Origin of iron and aluminium in large particles (> 53 µm) in the Crozet region, Southern Ocean. Marine Chemistry, 115 (1-2), 31-42. (doi:10.1016/j.marchem.2009.06.002 <http://dx.doi.org/10.1016/j.marchem.2009.06.002>). Article PeerReviewed 2009 ftsouthampton https://doi.org/10.1016/j.marchem.2009.06.002 2023-08-03T22:19:18Z Natural iron fertilization processes are occurring around the Crozet Islands (46°26?S–52°18?E), thus relieving the water masses from the normally encountered High Nutrients Low Chlorophyll (HNLC) conditions of the Southern Ocean. During austral summers 2004/2005 and 2005/2006, iron and aluminium concentrations were investigated in large particles (> 53 µm) collected from just below the mixed layer at stations under the influence of island inputs, and also in adjacent HNLC waters. These large particles are anticipated to sink out of the mixed layer, and to reflect the net effects of input and cycling of these elements in the overlying mixed layer. Labile and refractory fractions were determined by a two-stage leaching technique. Data showed that water masses downstream of the islands were enriched in total iron and aluminium (0.25–2.68 nmol L? 1 and 0.34–3.28 nmol L? 1 respectively), relative to the southern HNLC control sites (0.15–0.29 nmol L? 1 for Fe and 0.12–0.29 nmol L? 1 for Al), with only a small fraction (typically < 1%) being acid leachable in both environments. Particulate iron predominantly derived from the island system represents a significant fraction of the total water column iron inventory and may complement dissolved Fe inputs that help support the high summer productivity around the Crozet islands. Article in Journal/Newspaper Crozet Islands Southern Ocean University of Southampton: e-Prints Soton Austral Southern Ocean Marine Chemistry 115 1-2 31 42 |
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Open Polar |
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University of Southampton: e-Prints Soton |
op_collection_id |
ftsouthampton |
language |
unknown |
description |
Natural iron fertilization processes are occurring around the Crozet Islands (46°26?S–52°18?E), thus relieving the water masses from the normally encountered High Nutrients Low Chlorophyll (HNLC) conditions of the Southern Ocean. During austral summers 2004/2005 and 2005/2006, iron and aluminium concentrations were investigated in large particles (> 53 µm) collected from just below the mixed layer at stations under the influence of island inputs, and also in adjacent HNLC waters. These large particles are anticipated to sink out of the mixed layer, and to reflect the net effects of input and cycling of these elements in the overlying mixed layer. Labile and refractory fractions were determined by a two-stage leaching technique. Data showed that water masses downstream of the islands were enriched in total iron and aluminium (0.25–2.68 nmol L? 1 and 0.34–3.28 nmol L? 1 respectively), relative to the southern HNLC control sites (0.15–0.29 nmol L? 1 for Fe and 0.12–0.29 nmol L? 1 for Al), with only a small fraction (typically < 1%) being acid leachable in both environments. Particulate iron predominantly derived from the island system represents a significant fraction of the total water column iron inventory and may complement dissolved Fe inputs that help support the high summer productivity around the Crozet islands. |
format |
Article in Journal/Newspaper |
author |
Planquette, Hélène Fones, Gary R. Statham, Peter J. Morris, Paul J. |
spellingShingle |
Planquette, Hélène Fones, Gary R. Statham, Peter J. Morris, Paul J. Origin of iron and aluminium in large particles (> 53 µm) in the Crozet region, Southern Ocean |
author_facet |
Planquette, Hélène Fones, Gary R. Statham, Peter J. Morris, Paul J. |
author_sort |
Planquette, Hélène |
title |
Origin of iron and aluminium in large particles (> 53 µm) in the Crozet region, Southern Ocean |
title_short |
Origin of iron and aluminium in large particles (> 53 µm) in the Crozet region, Southern Ocean |
title_full |
Origin of iron and aluminium in large particles (> 53 µm) in the Crozet region, Southern Ocean |
title_fullStr |
Origin of iron and aluminium in large particles (> 53 µm) in the Crozet region, Southern Ocean |
title_full_unstemmed |
Origin of iron and aluminium in large particles (> 53 µm) in the Crozet region, Southern Ocean |
title_sort |
origin of iron and aluminium in large particles (> 53 µm) in the crozet region, southern ocean |
publishDate |
2009 |
url |
https://eprints.soton.ac.uk/68673/ |
geographic |
Austral Southern Ocean |
geographic_facet |
Austral Southern Ocean |
genre |
Crozet Islands Southern Ocean |
genre_facet |
Crozet Islands Southern Ocean |
op_relation |
Planquette, Hélène, Fones, Gary R., Statham, Peter J. and Morris, Paul J. (2009) Origin of iron and aluminium in large particles (> 53 µm) in the Crozet region, Southern Ocean. Marine Chemistry, 115 (1-2), 31-42. (doi:10.1016/j.marchem.2009.06.002 <http://dx.doi.org/10.1016/j.marchem.2009.06.002>). |
op_doi |
https://doi.org/10.1016/j.marchem.2009.06.002 |
container_title |
Marine Chemistry |
container_volume |
115 |
container_issue |
1-2 |
container_start_page |
31 |
op_container_end_page |
42 |
_version_ |
1775350217466445824 |